Papers - Flotation of Nonsulfides - Relative Floatability of Silicate Minerals. (With Discussion)

The American Institute of Mining, Metallurgical, and Petroleum Engineers
John Mark Patek
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
23
File Size:
1105 KB
Publication Date:
Jan 1, 1935

Abstract

Knowledge of the relative floatability of silicate minerals is increasing in importance as flotation is being applied to the concentration of nonsulfides. Many silicates are in themselves commercial products amenable to concentration by flotation. Moreover, the selective flotation of other nonsulfide minerals, such as cassiterite, depends largely upon the floatability of associated gangue silicates. Differences in floatability existing between the various silicates have not- been sufficiently appreciated; for example, the feldspars that differ greatly in floatability have generally been merely treated as "feldspar." It was the purpose of the work described in this paper to determine by experiment the differences in floatability between silicates; to investigate the causes for such differences, and to discover a means of predetermining approximate floatability without the necessity of experimentation. Determining Floatability The relative floatability of 20 silicates so selected as to represent all of the more common silicate types1 was obtained by flotation tests enumerated in Table 1. The mineral to be floated was crushed dry on a steel plate, and screened repeatedly during crushing through an 80-mesh screen in order to produce a sand with all grains as close to 80 mesh as possible. The sand was placed in dilute (6N) hydrochloric acid until free of soluble foreign material, and then washed with tap water about ten times in order to remove both acid and fines. The resultant product, which averaged 82 per cent plus 200 mesh, was floated in 50-gram charges in a 50-gram Denver celluloid flotation machine with 0.008 gram of terpineol, and from 0.01 to 0.05 gram of oleic acid in a solution acidified with sulfuric acid. The degree of separation of one mineral from another was determined by counting under a nlicroscope the grains of each mineral, both in the concentrate and in the tailings, and comparing their relative abundance in each. Unless the comparison showed a decided difference in amount,
Citation

APA: John Mark Patek  (1935)  Papers - Flotation of Nonsulfides - Relative Floatability of Silicate Minerals. (With Discussion)

MLA: John Mark Patek Papers - Flotation of Nonsulfides - Relative Floatability of Silicate Minerals. (With Discussion). The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1935.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account